Geochronology and geochemistry of Late Cretaceous-Paleocene granitoids in the Sikhote-Alin Orogenic Belt: Petrogenesis and implications for the oblique subduction of the paleo-Pacific plate
K2-E1 granitoids are identified at the southern end of the SAOB. Their magmas were derived from partial melting of a juvenile crust assimilated by ancient material. K2-E1 granitoids indicate the oblique subduction of the Paleo-Pacific plate.